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Lecture 4.3_Biogeography and Global Provincialism in Mammalian Distributions
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hello again Professor Jared rathel here
and this is lecture 4.3 in ABS 470 it's entitled
entitled
biogeography and Global provincialism
and mammalian distributions
so when we think about mammalian
distributions around planet Earth why is
it that we see mer mccophagus meaning
ant and Termite eating mammals on nearly
every continent on the planet
yet they're all different
how do scientists explain the abundance
of marsupials in Australia and South
America but their absence or scarcity on
Northern continents
why are there camels in Asia North
Africa and South America
what factors led to the present
distribution of primates from Japan to
Africa to South America so these are
biogeographical questions this lecture
is going to align with chapter 5 which
is entitled biogeography please note and
this is also in canvas but you may skip
the sections in your textbook entitled
biogeographic inference as well as the
section simply called examples
biogeography is the study of the
distribution of organisms both living
and extinct around our planet the most
basic unit of biogeography is the
species range that is to say the
complete area over the planet over which
individuals of a particular species
occur so as an example this is Puma
concalor common names include the
mountain lion the cougar the panther the
Catamount all the same species so Puma
concalor is distributed from British Columbia
Columbia
all the way down through the southern
tip of Argentina
as you likely recognize uh species
ranges are Dynamic they're not fixed in
time they're they're changing especially
as humans rapidly transform both the
surface of the planet as well as its
atmosphere our climate an endemic
species is one that's restricted in its
range only to a circumscribed area it's
only found there so for example we can
say that lemurs are endemic to
Madagascar they're only found in
Madagascar lemurs are not found across
the channel in Mozambique
hindemism is really important in
conservation biology because it helps us
identify biological hot spots regions
around the world that have really unique
flora and fauna that are worth
conserving like Madagascar a second
pattern of interest is known as disjunct
distribution so that simply means that
there's a gap in the range of related
species or some taxonomic claim so as
you already know
marsupials are abundant on the continent
of Australia and the island of Tasmania
as well as in South America and then we
have the Virginia opossum here in North
America you may also recall that the
oldest metatherian fossil yet recovered
is synodelphies which dates at 125
million years ago and was recovered in
Asia of all places
further the oldest confirmed marsupial
fossil recovered dates at 65 million
years ago and that's in North America so
it suggests that the ancestors of modern
marsupials dispersed from Asia to North
America and then down into South America
and we know that South America
represents the Cradle of marsupial evolution
evolution
marsupials then make their way across a
once green Antarctica and it may have
been just one colonizing species that
makes it to Australia some 50 million
years ago and the winner of that
sweepstakes their descendants are then
going to go on and fill almost every
conceivable mammalian ecological niche
in Australia
ecological biogeography it's going to
focus on the current distributions of
species but it's going to seek to
explain those distributions in terms of
community level interactions between the
species and their environment so one
common line of inquiry within ecological
biogeography is thinking about species
richness so that refers to how many
species are in the system in the region
and it leads to questions like why is it
that we see so many mammalian species
distributed between about 23 degrees
north of the equator down to 23 degrees
south in this Tropics in the tropical
band here so think about out the Amazon
rainforest or East Africa so you can see
species richness for mammals is quite
High uh in these these regions uh
whereas places like Antarctica they have
very few mammals
okay further when we think about
ecological biogeography we can think
about islands and why certain Islands
have relatively High species richness
compared to other Islands so and we're
going to come back to Island
biogeography but it has to do with the
size of the island as well as its
distance from the mainland
so answers to ecological biogeographical
questions are going to involve evolutionary
evolutionary
adaptations so ecological biogeography
is going to frequently entail studying
patterns of morphological
physiological and or life history
variation among mammals in different
places if we tabulate the number of
species and major clades of virtually
any group of animals or plants for that matter
matter
they occur in different Continental
regions of the earth and in doing so two
patterns are going to emerge first
different regions Harbor distinct
taxonomic assemblages so there's there's
endemism on a worldwide scale so think
kangaroos they're endemic to Australia
Gibbons in Southeast Asia sloths in
South and Central America
second pattern there are dramatic
differences in species richness amongst
the Continental regions some regions
represent centers of diversity While
others simply do not so these
observations together with knowledge
about phylogenetic or evolutionary
relationships demonstrate this
provincialism these provinces of Life on
planet Earth and it's a pattern that's
evident in the tetrapod fossil record
since the early Mesozoic some 250
million years ago it was way back in
1876 that the famous naturalist who
worked out both the mechanics and the
profound implications of natural select
action independent of Darwin Alfred
Russell Wallace
he's the first to divide the world up
into faunal regions for which he
identifies six regions each with a
distinct assemblage of species those are
the pale Arctic the knee Arctic the
neo-tropical what he deems as the
Ethiopian Oriental and Australian
so Wallace noted that although the
distance between the islands of Bali and
lombok in Indonesia is only a little
over 20 miles in fact on a clear day you
can see from Bali to lombok from one
Island to the next
the faunal assemblages on those two
islands are Worlds Apart so
Bali and everything north of what has
now been deemed Wallace's line
everything up here is Asians part of the
Oriental species assemblage so think uh
crab eating macaques meanwhile
everything's south of Wallace's line is
Australian so think about tree kangaroos
on Papua New Guinea all right you know
the drill please put me on pause and
check out Wallace Darwin's forgotten
Frenemy which is embedded in canvas
thanks next I'm going to take you on a
really quick tour of Wallace's sixth
faunal regions so for each of the
regions I'll explain where it's at on
the planet the major biomes that
comprise each region and then I'll
highlight any endemic families in the
region that is to say families of
mammals that are found in that region
and no place else
so we'll begin with the pale Arctic this
is the largest of the faunal regions and
it consists of the old world that is to
say Europe Russia and Northern China
it's separated from the Ethiopian region
uh by the deserts of the Middle East
it's separated from the Oriental region
by the Himalayan mountains which are
pretty formidable barrier and then it's
separated from the knee Arctic region by
the bearing straight
so there's an Eastward band of tiger uh
coniferous forest that's going to run
about 60 degrees north latitude
let's see the southwestern pale Arctic
includes the Mongolian steps
while there's temperate deciduous forest
and Chaparral forests in Europe and then
the pale Arctic is home to just one
endemic sub-family the blind mole rats
shown top left
the pale Arctic mammals represent a
mixture of meat Arctic
Ethiopian as well as Oriental elements
so think
servids bovids
ersids and felids but there are
certainly unique lineages uh within
these families so uh the bactrim camel
shown here or the Siberian tiger uh
bottom middle or the adorable giant
panda the knee Arctic extends from
Beyond the Arctic Circle here in
Northern Canada all the way down to the
central Mexican plateau and it's going
to include the island of Greenland the
knee Arctic is separated from the pale
Arctic as mentioned on the previous
Slide by the bearing straight
and the knee Arctic is separated from
the neotropics uh by this Central
American transition zone uh this
tropical uh rainforest like the pale
Arctic the knee Arctic consists of
tundra up north and tiger coniferous
forest there's also deciduous forests on
our Eastern Seaboard as well as
grasslands and then uh Chaparral forests
and deserts where we live in the Southwest
Southwest
many of the families that we find in the
knee Arctic also exist in the pale
Arctic because these two regions have
often been connected uh by the Bering
land bridge uh which multiple times uh
in the past have connected uh Siberia to
Alaska there are relatively few
mammalian families that are endemic to
the knee Arctic but there are two and
those are the families of the pronghorn antelope
antelope
as well as the mountain Beaver the Neo
Tropics or the nootropics extends from
Central Mexico all the way down to the
tip of South America the region is
mostly isolated it's surrounded by
oceans uh but it's Northern boundary
roughly coincides with a transition uh
from Zurich or dry subtropical desert to
moisture tropical forests okay so that's
a tough boundary uh to cross
tropical wet Forest of the Amazon
dominate the neotropics with grasslands
and deserts to the south of the Amazon
and then Alpine habitats that are
associated with those High impressive
Andes mountains along the western margin
of South America the neotropics are a
true Center of diversity they have large
numbers of mammal families and many of
them are endemic so think uh guinea pigs
the cavids this is a wild guinea pig
here uh sloths the two and three-toed
sloths that we've covered uh New World
monkeys we're going to cover primates
next we spent quite a bit of time
thinking about the opossums the many
different opossums that are found in
South America and then lastly the
selenodons are endemic to the region and
they're found in the Caribbean moving
over to the continent of Africa uh
Wallace deemed this final region the
Ethiopian region and it's going to refer
to sub-Saharan Africa that is to say the
portion of the African continent which
is south of the expansive Saharan Desert
including the island of Madagascar so
the Saharan Desert and the deserts of
the Middle East that's going to form the
transition zone the boundary between the
Ethiopian faunal region and that of the
pale Arctic the biomes in Africa there
is a massive swath of tropical
rainforest here uh in the Congo uh
southwestern Africa is characterized by
deserts so the Kalahari Desert excuse me
uh we've got Savannah in Eastern Africa
and then over in Madagascar there's rain
forest on the east side and Savannah on
the west and those habitats are going to
run parallel along that Island
so there is a great diversity of mammals
in Africa and it's been attributed in
part to restriction of plyo pleistocene
Extinction so just we didn't see the
extinctions uh in the plyocene and
pleistocene in Africa that we saw in
other regions like North America
further there's been a relatively recent
diversification of moderately large
bodied animals in Africa so indomism in
Africa and the Ethiopian region is
really high on the island of Madagascar
which you probably guessed uh endemic
species to Madagascar include the Lemurs
which we'll talk about next when we talk
about primates as well as these really
cool bats uh they are called uh sucker
footed bats and if you look closely at
their hands their little suction cups to
adhere to the surfaces of leaves so
really cool endemic bats in Madagascar
as well as the 10 Rex are endemic uh to
this region on the mainland uh Ethiopian
endemics include the gold in moles the
elephant shrews you remember we went
over those as well as the aardvark and
then there's an incredible uh radiation
of terrestrial Set artiodactyls uh
hoofed animals uh like uh the wildebeest
which we'll cover later in the semester
the Oriental region is comprised of the
Indian subcontinent
southeast Asia and the Malay archipelago
north and west of Wallace's line
so the Oriental region the primary biome
is tropical rainforest and it is a
stunningly beautiful Forest as somebody
who spent quite a bit of time in Thailand
Thailand
the mammal diversity in the orient is
quite High there are five endemic
families including the dermoptera the
kalugos and the scandentia the tree
shrews both of which we've just covered
as well as the aptly named hognose bats
the Gibbons and the Tarsiers uh both
primates that will cover next
and then the last point that I'd like to
make is the Oriental region is really
across roads and so it's going to
consist of Ethiopian families
um so the Asiatic lion lions evolved in
Africa uh the Asiatic lion was once
incredibly widespread uh sadly there's
only a few hundred uh Asiatic Lions left
their marooned uh in the gear Forest of
India and then uh the ursids this is a
pale Arctic family the bear family an
oriental species is the sun bear which
was also once widely distributed uh but
now the sun bears main stronghold is in
Cambodia the Australian final region
obviously includes the continent of
Australia as well as New Guinea and
Tasmania so it's bounded by AI Wallace's
line here in the Northwest which we've
discussed and then it's surrounded by
oceans which means it's highly isolated
there is a variety of biomes in
Australia it's mostly desert but we have
tropical rainforest in northeastern
Australia and places like Cairns and
Townsend as well as in New Guinea there
are temperate deciduous forests in the
south east there's Chaparral forests in
the South there's temperate rainforests
in eastern Tasmania so as you likely
recognize because Australia is so
isolated uh it's going to share very few
of its mammalian families with other
areas so endemism is quite High
endemics include the monotreams like the
spiny echidnas and the duck build
platypus as well as many marsupial
orders including uh the dazzy
euromorphia like this tiger Coral uh the
notoricta morphia like the marsupial
mole here the uh Bilby or the
rabbit-eared a Bandicoot uh the die
Proto dantia which are the Kangaroos and
the wallabies
so the only recent route of exchange for
Australian mammals is by Crossing
Wallace's line and there's two euthyrian
groups that have done just that the bats
and the murid rodents who we will talk
about so they've invaded a good example
is this species here this is the Gould's
mouse named after Stephen J Gould it was
thought to be extinct for 150 years but
was recently found thriving on numerous
small islands off the western coast of
Australia so that's your feel-good story
for the lecture and our final faunal
region is actually not one that was
identified by Wallace but it's pretty
important with respect to mammalian
distributions and that is the oceanic
faunal region it's comprised of mammals
that live on isolated did remote Islands
far from Continental land masses so
think about the Hawaiian hoary bat or
these really beautiful rats this is the Slender
Slender
slender-tailed Cloud rat from the island
of luson in the Philippines
so it's going to include insular species
as well as our aquatic species those
living close to coasts like the manatees
and the dugongs as well as pelagic
species fully marine species that live
out in the open ocean
so Oceanic Islands particularly those
that are volcanic in their origin they
tend to have very few mammal species
only those mammals that could reach
there uh by wind wave or Wing
um so in Hawaii for example there's only
two endemic mammals the Hawaiian hoary
bat as well as the monk seal those
islands that do have mammals they're
mostly bats and small rodents or mammals
that have
been dispersed to the region By Us by
humans it's their dispersal has been
facilitated by humans so think about our
menageries so pigs goats uh the Norway
ship rat that's Road everywhere with us
around the planet
among the Marine groups we know the
serenians the manatees and the dugongs
they occur along tropical coasts uh the
pinnipeds like these sea lions they're
gonna breed on packed Ice uh in the
Arctic and uh Antarctic regions as well
as near shore rocks or coastal areas and
then we have the cetaceans uh like this
beautiful breaching humpback whale and
uh these spinner dolphins which are
amazing to see
these are pelagic species meaning
they're denizens of the open ocean the
suggestion that the continents of planet
Earth drift over vast periods of time
was actually first proposed way back in
1915 mean by Wagner but it wasn't
accepted until the 1960s because up
until that time there was no geological
mechanism known that could account for
such movement plate tectonics is going
to provide that mechanism so the Earth's
crust including the continents and the
ocean floor is made up of Rocky plates
that are actually floating on denser
partially melted molten mantle Rock
there are some 10 of these major plates
and then there are numerous smaller
plates they're separated from one
another uh by ridges trenches and faults
so as heat from Earth's core
radiates outward it creates convection
currents right uh in this viscous mantle
Rock which is going to move these land
masses so here's a really nice
visualization created by the California
Academy of Sciences that demonstrates
the breakup of the supercontinent of
Pangea and into uh godwana land and then
the movement of our continents to their
current positions so this abiotic
process happened over the past 200
million years really important with
respect to mammalian Evolution because
it's going to create isolation and then
adaptive radiations and it's going to
really be the a driver for this
provincialism these centers of diversity
that we've been discussing that really
shape mammalian distributions today so
please take the two minutes uh and check
out this visualization
the climate or the long-term weather
patterns of a particular area on planet
Earth is the result of interactions
between sunlight the atmosphere the land
masses themselves as well as ocean
currents so a portion of the sun's
infrared radiation that reaches the
Earth is reflected back off the surface
and then it's trapped by carbon dioxide
and other greenhouse gases like methane
this blanket of gases in the atmosphere
is what creates the Greenhouse Effect
and it makes our planet livable inhabitable
inhabitable
but as I'm sure you're aware the amount
of CO2 in our atmosphere is rapidly
Rising so we're currently at 420 parts
per million that's the most CO2 in our
atmosphere in the past 400
000 years as measured by Antarctic Ice
cores so 400 000 years that's longer
than we've even been homo sapiens
although the Earth is warming at an
unprecedented rate today at several
times in Earth's history levels of
greenhouse gases fell and continents
occupied positions that blocked the flow
of warm equatorial ocean water to the poles
poles
and we got ice ages so for example in
the Carboniferous much of Southern
godwana was covered by glaciers which
had dramatic impacts on the pelicosaurs
and I hope you remember them way back
from module one
more recently
from the mid Maya scene on which is
about 15 million years ago the world
became cooler and drier until roughly
two million years ago when it was
plunged into the pleistocene Ice Age so
glaciation during this period was most
dramatic in the knee Arctic in North
America which you can see here where
there were these giant ice sheets these
incredible glaciers that covered most of
modern Canada and the northern United
States and it shifted the tundra and the
Taiga the coniferous forests Southward
between about 1.7 million years ago up
until as recently as 10 000 years ago
continental glaciers Advanced and then
retreated at least 4 four times giving
rise to a cycle of glacial and then
interglacial periods that culminated in
the recent distributions of many modern
mammals that are still responding to the
last glacial Retreat and now of course
the big question is are they going to be
able to respond to anthropogenic climate
change the term dispersal has two
closely related meanings in ecology the
first is when individuals or small
groups of individuals leave their natal
area the place where they're born and
raised to go and breed elsewhere so
think about young male wolves that
disperse from their natal pack to form
their own new pack so these types of
dispersals they're going to occur within
the lifetime of an individual organism
and we refer to this as ecological dispersal
dispersal
dispersal in the sense that we're
interested in today in the biogeographic
sense refers to a species
expanding its range so species dispersal
species dispersal can be passive
dispersal so think rodents rafting to an
island and then they hit the sweepstakes
and they land on this new island with no competition
competition
or species dispersal can be active so
that's when individuals of a species
actively disperse via a corridor route a
corridor route is one that provides
minimal resistance to the passage of
animals between two areas whereas a
filter route is going to do just that
it's going to filter out some animals
it's only going to allow some animals to
pass through the filter route so for
example flying bats are really good at
getting through filters the filter of
Wallace's line as well as animals that
have really large home ranges so think
about Puma con color
from British Columbia all the way down
to South America
um so a great example of a filter route
is the Panamanian land bridge that forms
between North and South America about
3.5 million years ago
and facilitated the Great American
biotic interchange so this Ted Ed is
going to do a very nice job of breaking
that down for you so check it out in the
pliocene about three and a half million
years ago this land connection between
North and South America was
re-established by the emergence of the
Isthmus of Panama right here which is
going to initiate
extensive dispersal of mammals between
the two continents so it's important to
note Panama was initially Savannah very
similar to Savannah habitats in the
North and the South so initially it's a
corridor for some mouth were dispersing
mammals such as Horses and deer as well
as Savannah dwelling mammals from South
America like the glyptodons and the
ground sloths however Panama is going to
develop into a tropical rainforest
during the pleistocene and then it's
going to be less of a corridor and more
of a filter which is only going to allow
some animals through
so from the north
rabbits and squirrels rodents the
canaans the Bears the raccoons they were
able to cross this filter and make their
way into South America whereas
whereas
shrews and beavers and pronghorns did
not make it
okay thinking uh uh the other way
um porcupines and opossums were able to
invade uh North America along with the
nine banded armadillo however most
armadillos and anteaters and the
tropical sloths uh were not able to make
it through that filter so the difference
between a corridor and a filter route
really nicely exhibited uh By the Great
American biotic interchange which was
initially a corridor and then became
more of a filter just as Extinction is
going to reduce the species richness of
a clade evolutionary diversification is
going to increase species richness so
diversification in this sense is nothing
more than speciation but the most
noteworthy cases of speciation those in
which it happens very rapidly and we see
this incredible explosion of new
descendant species in a geographically
restricted area we're going to refer to
these as adaptive radiations
so some spectacular examples of adaptive
radiations when
um you know one species makes it to a
new area and we see this incredible
flowering of new species include the
Lemurs on the island of Madagascar of
which there are over a hundred species
there's my favorite the II the new world
monkeys another uh wondrous adaptive
radiation which we'll cover in our next
lecture and then of course the
Australian marsupials which we've talked
about at length of which there are over
240 species in these cases the ancestors
of these clades they disperse into this
new region and they encounter little
competition in this new range or they
get there and they out-compete the
residents uh that are in that Niche a
striking regularity in mammalian
phylogeny is the number of times that
ecologically similar species have Arisen
in different areas and from different
ancestors because of
convergent evolution so this is a topic
that I've discussed multiple times this
semester thus far for example
mircophagy which I discussed on the
first slide mammals that specialize on
eating ants and termites with its
specialized cranial morphine apology and
those elongated sticky tongues that's
evolved in six different mammalian
orders including the numbats pictured
here which are of the marsupial order
dazzy uromorphia uh the anteaters
there's a giant ant eater here which is
in the order pelosa the pangolins which
are the folidota the aardwolves and the
Order of Carnivora the aardvarks uh the
tubule Eden Tata and the echidnas which
are monotreams
so your semester Capstone project which
I will describe in detail later it's
going to allow you to explore convergent
evolution in much greater depth it's a
fascinating topic since the 19th century
a number of regularities have been noted
in the ways that mammals vary with
geography many of these patterns have
been codified as Eco Geographic
rules but as your textbook notes none of
the patterns that I'm about to describe
are invariant there's a lot of
exceptions and some of these rules
really have questionable generality and
all of these rules are going to to be
the result of complex historical and
environmental factors
thus we call them rules but they're only
rules really in the loosest sense so
we'll start with the island Rule and
it's formulated on the observation that
small mammals on Islands tend to evolve
larger body sizes than their close
relatives their ancestors on the mainland
mainland
we see this insular or Island
gigantism on the island of Flores uh in
Indonesia with its giant rat so here's
the Flores giant rat
um considerably larger than rats that
are found on the Southeastern Asian mainland
mainland
conversely the island rule states that
large mammals are going to show the
opposite Trend so Island species usually
evolve smaller body sizes then their Mainland
Mainland
counterparts so the eco-evolutionary
underpinning goes like this
for large mammals like elephants
resource limitations on small Islands
small land masses should be the most
intense selection pressure and therefore
it's going to favor reduced body size
there just isn't as much forage for
elephants on Islands so there's going to
be selection for smaller and smaller elephants
elephants
however smaller mammals when they arrive
on Islands they're going to have reduced
inter-specific competition I.E
ecological release which is going to
favor the evolution of larger body sizes
for these small mammals which are less
likely to experience resource
limitations uh because of smaller areas
that Islands represent so if we go back
to the island of Flores we see insular dwarfism
dwarfism
in pygmy elephants which are now extinct
and then what I find Most Fascinating
is uh insular dwarfism in
homophorensis The Hobbit which likely of
involved from much larger bodied Homo
erectus and this little hominid it may
have died out as recently as 50 000
years ago so it may have overlapped uh
with uh the First Peoples uh in
Indonesia this is such an amazing
discovery that I want you to take a few
minutes and just check this out it is
just so cool
one of the earliest
eco-geographic rules was that of Bergman
way back in 1847 and he observed that
body sizes of both mammals and birds
tend to increase with increasing
latitude mammals are going to get larger
as we move farther north and south away
from the equator
the argument underlying this latitudinal
size gradient is based on the superior
heat conserving capacity of larger
bodied endotherms so a typical large
mammal has a much lower surface area to
volume ratio they have more volume
relative to their surface than a small
mammal hence smaller surface area across
which to lose body heat at cold temperatures
temperatures
so this subspecies of red fox here this
is the Arabian Fox it has a much lower
body mass and a lot more surface area
relative to its volume which is going to
allow it to dissipate heat
um compared to
um this arctic fox which has is
considerably chunkier and has a larger
body mass and is better able to conserve
heat less surface more mass in those
Arctic temperatures
so uh Blackburn and Hawkins uh from 2004
this is figure
5.18 in your textbook uh they found uh
that average annual temperature is the
strongest predictor among six factors
they evaluated
um in predicting average log body mass
uh in North American mammals okay so
here are these really cold regions and
you can see the mammals tend to be much
larger bodied and as average temperature
warms uh mammalian body sizes get
smaller so this is a negative uh
polynomial model extending bergman's
reasoning about
thermoregulatory adaptations in
endotherms in 18 177
177
Alan uh proposes this rule that mammals
as well as Birds again living in cold
climates have shorter appendages than do
their close relatives living in warmer
environments so long Limbs and Tails and
certainly ears they're going to increase
the surface area for heat dissipation in
mammals which is adaptive as a cooling
mechanism in hot dry environments like
the Sonoran Desert certainly appears to
be the case in uh jackrabbits in
comparison to Arctic hairs in
1883 a gloeger noticed an apparent
correlation between the plumage color of
closely related Birds and the humidity
levels of their habitats with birds with
darker feathers more frequently found in
human environments and birds with
lighter feathers more likely to exist in
dry areas
so in mammals the rule would apply to
their pillage their fur color so for
example white light colored polar bears
inhabiting the very dry Arctic in
contrast with the dark brown grizzly
bear and the humid or at least
relatively human boreal forests of North
America and Eurasia so gloeger's rule
has been documented in primates uh but
other than that it's generality it
appears quite Limited
Rapaport in 1982
1982
noted that the
latitudinal breadth of a species range
tends to increase as we move from
equatorial species up in Latitude
towards the poles so for example
consider the Y distribution of the
Caribou range of her tyrandis right
really widely distributed species
obviously at high latitudes uh around
the Arctic Circle in comparison to the
very restricted range of the elds deer
pictured here which lives in tropical
southeast Asia much closer to the Equator
Equator
so it's argued uh that species living at
high altitudes like the Caribou they're
adapted to this relatively broad range
of seasonal environmental conditions
right so uh you know in June we've got
the Sun never setting and then um you
know obviously in December uh perennial
Darkness so these huge swings uh that
Caribou have to deal with in contrast
tropical species are adapted to a more
stable climate thus they may have
evolved towards more ecological
specialization and have narrower
distributions I'll conclude this lecture
with the latitudinal gradient in species
diversity so this is probably the first
Global ecological path pattern that was
described by naturalists so species
diversity I.E the number of species per
unit area is going to decrease as we
move away from the equator up towards
the poles
so for example there are less than 40
species of mammals that inhabit
latitudes above the Arctic Circle but as
we move towards the equator
mammalian species richness increases
and as we get all the way here to Costa
Rica we're gonna Peak at about 160
species of mammals that inhabit uh these
lush tropical Costa Rican rainforests so
there's quite a few hypotheses uh that
have been put forth to explain this uh
you know pretty
um solid observation that exists not
only in mammals but in a whole variety
of different taxa these hypotheses
aren't mutually exclusive and I just
wanted to go over two really quickly the
first is the out of Tropics model and it
posits that most mammalian clades
evolved originated in the tropics in the
tropics they experience low Extinction
rates so species tend to persist for
longer periods of time and from the
tropics they're going to move out and
colonize subtropical and temperate
regions as a function of distance
and then another argument is the
metabolic hypothesis and it's going to
argue that the higher primary
productivity of tropical habitats just
results in higher rates of speciation as
well as lower Extinction rates because
they're more stable in comparison to
temperate habitats when you think about
these habitats just during the
pleistocene with uh you know glaciers uh
advancing and then retreating we see a
lot of variability over time and with
that I will bring lecture 4.3 to a close
I am super excited about our next
lecture so I'll be discussing mammalian
mating systems and parental investment
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